Can Switzerland Store Its Own CO₂ Underground? The Science Says No

A serene alpine lake with wooden boats docked at a pier, surrounded by snow-capped mountains and autumn-colored forests. A large red arrow points downward with “CO₂” written in red, accompanied by a leaf icon, symbolizing carbon sequestration or CO₂ reduction in nature

New research reveals why the country’s geology makes underground carbon storage unfeasible and what alternatives might work instead

Switzerland, like most other countries, is in a race against time to reach its net-zero emissions goal by 2050, and finding ways to permanently store carbon dioxide (CO₂) is a big part of the challenge. 

This is because while renewable energy, efficiency improvements, and lifestyle changes can reduce emissions, some sectors — like waste incineration — are hard to clean up entirely. That’s where carbon capture and storage (CCS) comes in. 

But where does the captured CO₂ go? I’ve talked a lot about carbon sequestration and storage here, and most of the solutions involve using vegetation to capture CO₂, seizing the photosynthetic processes that allow them to grow

But this isn’t the only option available, and many countries have turned to underground storage, injecting CO₂ into rock formations deep beneath the surface. 

However, a new study set out to see if Switzerland could store its own CO₂ through in-situ mineralization, a process that permanently locks CO₂ into solid rock. Unfortunately, the results weren’t promising.

(left) Schematic illustration of the injection of CO2 dissolved in water into mafic and ultramafic rocks (Adapted from: Gislason and Oelkers (2014); Snæbjörnsdottir et al. (2020, 2014)); (right) Main steps in the in situ CO2 mineralization process (Adapted from: Campbell et al. (2022); Matter and Kelemen (2009); Gislason et al. (2010)) — Martin et al., 2025

How CO₂ Can Become Rock

The idea behind in-situ mineralization is simple: inject CO₂ dissolved in water into underground rocks rich in minerals like calcium and magnesium, and chemical reactions will turn the gas into solid carbonate minerals (see the figure above as a reference). 

This isn’t something completely new, though. The approach has already worked in places like Iceland, where the CarbFix project has successfully stored thousands of tons of CO₂ in basaltic rocks. 

This is because, if the conditions are right, the process happens quickly — within a few years — locking the carbon away permanently.

But for it to work, the underground rocks have to meet very specific criteria. They need to be rich in reactive minerals, have enough porosity and permeability to allow CO₂-rich water to flow through, and be located at the right depth and temperature for mineralization to occur efficiently. 

As you can imagine, that’s a tough combination to find.

The classification of igneous rocks is based on the relative abundances of minerals. Mafic rocks (e.g., Basalt) and ultramafic rocks (e.g., Peridotite) have distinct mineral compositions. Under high temperatures and pressures deep within the Earth, the mineral composition, texture, or chemical properties of preexisting rocks (such as igneous rocks) can be altered, resulting in the formation of metamorphic rocks (e.g., Metabasalt, Serpentinite) (Adapted from: Grotzinger and Jordan (2014); Panchuk (2019)) — Martin et al., 2025

The Search for Swiss Storage Sites

Researchers from ETH Zurich scoured geological maps, analyzed rock compositions, and identified potential storage zones across Switzerland, particularly in the Alps. 

The best candidates were mafic and ultramafic rock formations which contain basalts, serpentinites, and peridotites known for their ability to store CO₂ through mineralization.

At first glance, it looked like Switzerland had the right rock types. But the closer researchers looked, the more problems emerged.

Why It Won’t Work

I know what you’re thinking. If they have the right type of rocks, why won’t this work in the Alps like it did in Iceland?

Well, the biggest roadblock is Switzerland’s geology. Unlike Iceland’s young, highly fractured basalt, Swiss alpine rocks are old, heavily deformed, and metamorphosed

This means that, over millions of years, heat and pressure have altered the rock structure, closing up fractures and reducing porosity and permeability to almost nothing. In simpler terms, the rocks are too compact to allow CO₂-rich water to move through them efficiently. 

As you can imagine, if the fluid can’t circulate, the mineralization reactions won’t happen.

Image 1

Diagram showing the methodology used to screen, classify, and characterize rock formations based on their potential to store CO2 through in situ mineralization by injecting CO2 dissolved in water — Martin et al., 2025

Another challenge is temperature. In-situ mineralization works best between 90°C and 185°C, but in Switzerland, you’d have to drill more than 3,500 meters deep to reach those conditions. That makes the process expensive and technically complex.

Then there’s the water problem. Mineralization requires a huge amount of water — about 25 tons of water per ton of CO₂ stored. Switzerland already faces water management challenges, with competing demands from hydropower, agriculture, and industry. Diverting massive amounts of water for CO₂ storage could cause conflicts.

That said, even if these technical issues were solved, there would still be economic, legal, and social hurdles. 

Who would pay for the infrastructure? Would the public support CO₂ storage near their communities? What regulations would be needed to ensure safety? 

Because of these, and many other questions, the study concluded that, taken together, these challenges make in-situ CO₂ mineralization unfeasible in Switzerland — both in the near term and likely in the long run.

a) Location and surface extent of selected areas for potential CO2 storage through in situ mineralization. The different colors represent the different tectonic units/nappes in Switzerland (Map Background: swisstopo (2005)); b) Geological cross-section of the Tsaté nappe illustrating the complex structure and lack of stratigraphic continuity. The different colors correspond to the different rock formations. The target formations are metabasalts (dark green) and serpentinites (light green) (Modified after Marthaler et al. (2020)). Additional cross-sections of the Tsaté nappe are reported in Fig. 6 in the Appendix, with a complete list of the different rock formations — Martin et al., 2025

So Where Can Swiss CO₂ Go?

If Switzerland can’t store its CO₂ underground, what are the alternatives? 

Well, one promising option, according to the study, is storing CO₂ in deep saline aquifers, large underground water-bearing formations that can trap CO₂ safely. Researchers have already tested this near Zurich, and results suggest it could work. 

Another solution is exporting CO₂ to countries with better storage conditions, as Switzerland is already doing with Iceland’s CarbFix project.

The takeaway? Not every country can store its own CO₂ underground. While places like Iceland have ideal conditions for mineralization, Switzerland’s complex alpine geology makes it a poor candidate. 

That means Swiss climate policy needs to focus on alternatives — whether that’s improving international storage partnerships, investing in new carbon capture technologies, or simply reducing emissions at the source.

There’s no one-size-fits-all solution to carbon storage, but understanding what won’t work is just as important as figuring out what will. As we’ve talked about before, innovation through trial and error will help us through these environmental crises. 


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Best,

Sílvia P-M, PhD Climate Ages

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